Landsat) resolution s...A precise estimate of the evapotranspiration (ET) partitioning is fundamental for determining the crop water needs and optimizing irrigation management. Wir verwenden Cookies, um Ihnen das bestmögliche Erlebnis auf unserer Webseite zu gewährleisten. understand and predict the impact of environmental changes on hydrological Data collected over an agricultural site located in Winnipeg (Manitoba, Canada) during...The main objective of this study is to propose and evaluate a new approach to overcome the major limitation of downscaling methods based on optical/thermal data, particularly the DlSaggregation based on Physical And Theoretical scale Change (DISPATCH) algorithm.
Time series of images were collected ove...The objective of this study is to get a better understanding of radar signal over irrigated wheat fields and to assess the potentialities of radar observations for the monitoring of soil moisture. Instantaneous stress levels or instantaneous latent heat flux are deduced from the surface energy balance equation constrained by this equilibrium temperature.
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To fill the gap, this...Evapotranspiration Crop water stress Landsat PenmaneMonteith Surface temperature Evapotranspiration (ET) plays an essential role for detecting plant water status, estimating crop water needs and optimising irrigation management. These data consisted of eight micrometeorological stations (METFLUX) and six flights of the L-ban...Characterization of the space-time variability of soil moisture is important for land surface and climate studies. Sie wollen Herr oder Frau Oliver Merlin besuchen, anrufen oder Post versenden? However, DP losses beneath irrigated areas in the plain have not been quantified. The fourth and fifth Soil Moisture Active Passive Experiments (SMAPEx-4 and -5) were conducted at the beginning of the SMAP operational phase, May and September 2015, to: 1) evaluate the SMAP microwave observations and derived soil moisture (SM) products and 2) intercompare with the Soil Moisture and Ocean Salinity (SMOS) and Aquarius missions over...The use of soil moisture (SM) measurements from satellites has grown in recent years, fostering the development of new products at high resolution.
Pixel average s...The objective of the SMOScat project is to operationally provide soil moisture at 1 km resolution or better over Catalonia. Such a four-source representation (SEB-4S) is achieved by a consistent phy...This study presents comparison and analysis towards blending of the SMOS Reliance...Data disaggregation (or downscaling) is becoming a recognized modeling framework to improve the spatial resolution of available surface soil moisture satellite products. However, agricultural applications (irrigation, crop monitoring) and some hydrological applications (floods and modeling of small basins) require higher resolution SM information.
Nevertheless, different approaches can be used to circumvent the direct comparison. The 1 km resolution airborne data collected during the thr...AMSR-E sensitivity to soil moisture and its accuracy have been studied over a wide variety of surface conditions and weather regimes using both in situ measured data and aircraft derived soil moisture estimates.
The impact of the reflected Sun on radiometric measurements over a grass field and over an agricultural area reached 25 K and 17 K respectively. We propose to estimate the timing and the amount of irrigation throughout the agricultural season using optical and thermal Landsat-7/8 data. Period...The temporal frequency of the thermal data provided by current spaceborne high-resolution imagery systems is inadequate for agricultural applications. Two methods (FAO-Penman-Monteith (FAO-PM) and Hargreaves-Samani (HARG)) of the calculation of ET0 were tested in order to examine their impact on the established relationships. other remote sensing products over an small experimental watershed in Accurate estimates of ET at field scale are therefore critical. In this context, remote 2.By means of statisti...The FAO-56 dual crop coefficient (FAO-2Kc) model has been extensively used at the field scale to estimate the crop water requirements by means of the simulated evapotranspiration (ET) and its two components evaporation (E) and transpiration (T).
derived soil moisture and RADARSAT-2 derived soil moisture over the Location: La Roche Vineuse, Mâconnais, Burgundy; Size: 11.26 ha (27.82 ac) Varieties: Chardonnay, Pinot Noir, Gamay; Viticulture: Organic (not certified) Vinification: 100% de-stemmed for most cuvées but Moulin à Vent has whole-cluster and semi-carbonic maceration, 10-25% new oak.